The Westman Islands, or Vestmannaeyjar, are an archipelago of 15 islands and 30 rock stacks off the South Coast of Iceland. Aside from their incredible natural beauty, the islands have the world’s largest population of nesting puffins in summer, and a fascinating history.

History of the Westman Islands

The history of the Westman Islands is as dark as it is intriguing, beginning at the very start of Iceland’s history, with the first family to settle here.

The first person renowned for permanently settling Iceland was a man called Ingólfr Arnarson (although it should be noted that he hardly came alone; he was accompanied by his wife Hallveig Fróðadóttr and several slaves). His half-brother joined him in the country, a few years later, but met his death at the hands of two of his own captured men.

These slaves attempted to flee and hide, to escape Arnarson’s vengeance. They reached the Westman Islands, but unfortunately, were found by ‘Iceland’s father’ and killed in retribution.

The islands since have been named after these men; they were Irish slaves, and at the time, the Irish were called ‘Westmen’, as Ireland was thought to be the westernmost landmass before Iceland’s discovery.

This brutal beginning would be a hint at the later events to occur on and shape the archipelago.

The largest island, Heimaey, was settled in the early era, and the people on it lived off the fertile oceans, puffins, and eggs. Life was challenging but manageable, until a terrible tragedy occured in 1627.

At the height of the Ottoman Empire, it was Barbary Pirates from Algiers who ruled the seas, and they managed to find their way to this little island. They took control of it for three days, before setting off back home with 237 slaves.

The vast majority of these lived out the rest of their lives in bondage, though some were ransomed back in 1638.

The trials of the voyage and their captivity was captured in a novel by a priest who managed to escape in 1628.

Unfortunately, this was not the last major calamity to befall the islands.

In the 20th Century, it seemed that the Westman Islands had overcome their hardships, modernising and better connecting to the mainland. That, however, was to be overturned in 1974.

At 01.55, on January 20th, a fissure tore open in the middle of the town of Heimaey and the previously unknown Eldfell volcano began to violently erupt. In hours, it had torn across the island, spurting fountains of lava height in the air and pouring noxious gasses into the atmosphere.

Unbelievably, however, no-one was killed. There was an emergency plan for a situation such as this, and thankfully, storms the days before meant that the whole fishing fleet was docked in the harbour. The entire population of the island was taken to safety.

That is not to say, however, that the work was done. 5,300 peoples’ homes were in the town, and the Icelandic authorities were desperate to do what they could to help protect them. At the time, the US had a NATO base in the country, and their help was enlisted.

By pumping seawater onto the great lava fronts, it was possible to cool the molten rock, slow it, and change its direction.

This innovative, previously unused technique was particularly effective when it came to protecting the harbour. It seemed at one point that the eruption may have closed it entirely, effectively destroying the island’s economy, yet by spraying the lava, the harbour was actually enclosed more and improved.

When the eruption ended, the island slowly repopulated to about 85 percent of its previous population; about one fifth of the buildings were destroyed.

The town, however, now had a long stretch of new land to build a runway on, and a volcano in its centre to draw guests. Ever since, the Westman Islands have recovered as a popular tourist destination.

The Westman Islands today

Today, the Westman Islands attract thousands of visitors of years, for a variety of reasons. Many wish to visit the Eldborg crater and learn about the eruption in depth at the Eldheimar Museum. Others come for the incredible nature opportunities.

First and foremost amongst these are the chances for puffin watching. Ten million puffins nest in Iceland between May and September, and more of them come to the Westman Islands than anywhere else.

They nest in the cliffs, crags and sea-stacks, and can be easily seen by travelling on foot or by boat. Towards the end of the season, many of the pufflings get confused by the lights of the town as they try to make their way to the ocean, and end up in the streets; it is thus a local tradition amongst the children to collect them and throw them in the sea.

Some business-savvy young ones used to even collect them up, and ‘sell’ them to tourists to release.

The puffins are just one of the thirty or so species that nest on the islands, but by far the most abundant.

The Westman Islands also boast some of the best whale-watching opportunities in the country, with Fin, Minke and Humpback Whales seen often in summer, and Orcas throughout the year.

Skógafoss is one of Iceland’s biggest and most beautiful waterfalls with an astounding width of 25 meters (82 feet) and a drop of 60 meters (197 feet).

Due to the amount of spray the cascade produces, at least one rainbow is present any time the sun emerges from behind the clouds.

Located on the Skógá river, this mighty cascade is clearly visible from Route 1 and is an excellent place to stop and stretch the legs while travelling Iceland’s South Coast. The river below Skógafoss holds a large char and salmon population and is thus a favourite spot for fishermen in the summer.

The land underneath the waterfall is very flat, allowing visitors to walk right up to the wall of water. This will get you drenched, although, on a summer’s day, it can be quite tempting.

Skógafoss can also be viewed from the top as a steep staircase leads to an observational platform above the cascade. Many nesting seabirds can be found on the route up.

Geography

Skógafoss is located near the small village of Skógar, south of the Eyjafjallajökull glacier volcano. There you’ll find the Skógasafn folk museum, an open-air museum with both old wooden houses and turf houses, as well as a regional museum with various artefacts from this area.

A part of the Skógasafn Regional Museum is the Museum of Transportation, which showcases the history and evolution of transportation, communication and technologies in Iceland. There, you can see how this nation evolved from the age of the working horse to the digital communications of the 21st century.

The Skógasafn museum also includes a café and a museum shop, and in the village of Skógar, you will find both a hotel and a restaurant.

At the eastern side of Skógafoss, you will find one of Iceland’s most famed hiking routes; the Fimmvörðuháls pass. The 22 kilometre (14 miles) trail takes you along Skógá river, between two glaciers, Mýrdalsjökull and Eyjafjallajökull, before ending in the beautiful Þórsmörk valley.

Skógafoss is often visited alongside the waterfall Seljalandsfoss, which is just a little further along the South Coast. Both fall from cliffs of the same height, and while Skógafoss is much more powerful, Seljalandsfoss has a cave behind it, which means it can be fully encircled. It is also next to a much lesser known but still awe-inspiring waterfall, Gljúfrabúi.

Folklore

A gold ring is on display at the Skógasafn museum. According to legend, the ring is from a chest that was owned by Þrasi Þórólfsson, one of the first Viking settlers in the area, who by some accounts was a giant. Folklore states that before his death in 900 AD, Þrasi buried a chest filled with gold in a cave behind Skógafoss waterfall.

Many attempts were made to retrieve the chest after Þrasi’s death, and years later, locals managed to grasp a ring on the side of the chest. As they pulled, the ring broke off, and the treasure was lost forever. The ring was then given to the local church before it made its way to the museum.

Seljalandsfoss is a waterfall that can be fully encircled, situated on the South Coast of Iceland with a drop of 60 metres (200 feet).

Due to the waterfall’s close proximity to the Ring Road and impressive natural features, it is one the country's most famous and visited falls. Majestic and picturesque, it is one of the most photographed features in all of Iceland.

Geology and Surroundings

Seljalandsfoss waterfall, part of the river Seljalandsá, has its origins underneath the glacier Eyjafjallajökull. The volcano beneath this ice cap was the one that erupted in 2010 and caused havoc at airports across Europe.

The cascade of the falls is relatively narrow but falls from a tall cliff that once marked the country's coastline, the sea is now located across a stretch of lowlands and is visible from the site.

The most distinguishing feature of Seljalandsfoss is a pathway that stretches all the way around it. The cliffs behind the falls have a wide cavern, and rocks and paths allow guests to fully encircle it in summer.

Though a mesmerising opportunity, visitors should be prepared to get dampened due to the perpetual mist of the falls, which also tends to make the rocks of the pathway slippery.

Floodlights have been set up on both sides of the waterfall, which impressively illuminate the scene during the night when the midnight sun is not out. The lights were installed in 2001 due to the growing popularity of the falls as a tourist destination.

After visiting Seljalandsfoss, it is common for visitors to continue north to the waterfall Gljúfrabúi, which is found partially hidden behind a rock face. Because of Seljalandsfoss extreme popularity, Gljúfrabúi is widely considered the hidden gem of the scene, as it is too often overlooked.

Seljalandsfoss is also usually visited alongside the nearby Skógafoss. The waterfall falls from the same height, and while it cannot be encircled, it is much more powerful and steeped in the legend of a giant’s hidden treasure.

Visitor Centre Controversy

In 2017, it was announced that a visitor’s centre was to be constructed near the falls. The design of the building indicated that it would be seven metres (23 feet) high and 2,000 square metres (21,500 square feet) in size. Landowners in the area opposed to the idea, proclaiming that the centre would greatly alter the natural appearance of the waterfall’s renowned scenery.

The project has neither been fully approved nor wholly cancelled, with ideas surfacing of either significantly reducing the size of the construction, or moving the visitor centre’s location further away, for instance to the nearby farmstead Brekkuhorn.

Seljalandsfoss in Popular Culture

Along with a multitude of South Iceland’s most famous natural attractions, Seljalandsfoss can be seen in Justin Bieber’s music video for his song ‘I’ll Show You’. Please enjoy the video without emulating any antics that will endanger yourself or the environment.

The waterfall was also a featured waypoint during the first leg of the sixth season of The Amazing Race, an American reality TV series.

Hekla, nicknamed ‘the Gateway to Hell’ in the Middle Ages, is one of Iceland’s most explosive, unpredictable and powerful volcanoes. It has erupted twenty to thirty times since settlement, and remains active to this day.

Geography of Hekla

Hekla is located in the south of Iceland, just north of the country’s most famous volcano, Eyjafjallajökull, which last erupted in 2010, causing planes to be grounded and reporters to be tongue-tied for weeks. A dominant peak, standing at 1,491 metres tall (4,892 feet), it can be seen for miles around.

Hekla is part of a 40 kilometre (25 mile) rift, the most active part, called Heklugjá, being under the volcano itself. There are many craters at the peak, two of which are known to erupt more than the others.

Unlike Eyjafjallajökull and Iceland’s other most active volcano, Katla, Hekla does not sit underneath any significant glacier, meaning its eruptions should not cause ash clouds to the same degree. In spite of this, some have been so great that the ash produced was still enough to change the climate of the northern hemisphere for years.

Hekla has also produced one of the greatest lava flows of this millenium of any volcano in the world, at eight cubic kilometres. Approximately 10 percent of Iceland’s landmass was brought up by lava from Hekla.

History of Hekla

The first recorded eruption at Hekla was in 1104, and it was so great and significant that it drew attention across Europe; the effects it had on the weather, on people’s breathing, and on agriculture lasted for years.

This, however, was not the first time it had done so; undiscovered by man, it had contributed to a third of all volcanic ash across northern Europe for the past seven millenia.

It would not significantly erupt again until 1300, although it had been recorded going off several times in between; one of the most notorious things about Hekla is its unpredictability, sometimes exploding within a decade of its last eruption, sometimes laying dormant for nearly a century.

For this reason, the farms around it were largely abandoned, partly explaining why today there are few settlements in Iceland’s south.

Further serious eruptions occurred in 1693 and 1845 with international consequences, but none as significant as the one that began in 1947. Lava bombs weighing over 20 kilograms (44 pounds) landed 32 kilometres away; some as large as 50 square metres (538 square feet) were thrown a kilometre. It took just 52 two hours before the enormous cloud of ash was covering Helsinki.

It would be thirteen months before the eruption stopped, ebbing and flowing with power, but constantly pouring ash into the atmosphere, poisoning crops and livestock.

It is likely many died of respiratory problems as a result, but Hekla even directly killed one person. A scientist filming the great lava flows from the crater, some of which were 15 metres (49 feet) tall, was struck by a block of lava.

Hekla erupted again in 1970 for two months, but since has only gone off for a few days at a time, in 1981, 1982, 1991 and 2000.

Though the 2000 one seemed inconsequential, it was later discovered that it proved that Hekla was even more frightening than was already thought. The remains of a pyroclastic flow, the most dangerous element of an eruption, where searing ash and rock travel at enormous speeds and raze all they meet, had occured for over five kilometres (three miles).

Hekla today

In spite of its volatile nature, Hekla can still be considered a safe place to visit; there are hiking opportunities all around it, and some tour operators embark in super jeeps journeys to its slopes. Visitors should not be afraid of the volcano’s potential, just aware of it.

Of course, before heading to Hekla if travelling without a guide, ensure you check the meteorological office’s website to ensure that there are no alerts that an eruption may be imminent. The volcano is monitored constantly.

In spite of this, Hekla remains as unpredictable as it ever was, and visitors are warned that in spite of every good measure, there is always a chance an eruption could start without being noticed.

Volcanologists also warn that it is overdue, and due to this volcano’s patterns, the warning time between knowing an eruption is imminent and it occurring will often be just an hour or less.

Hengill is an enormous mountain in south-west Iceland, covering an area of about 100 square kilometres. It is a vital source of energy for south Iceland

Energy at Hengill

Hengill is an active volcano, although there has not been an eruption here for about 2,000 years. In spite of that, there is still lava close to the surface, evidenced by the steaming fumaroles and many hot springs dotted across it.

Iceland’s electricity and heated water comes from entirely renewable sources, taken from places such here. There are two power stations harnessing the energy potential at Hengill, called Nesjavellir and Hellisheiði.

Popular sites at Hengill

The energy beneath Hengill does not only help Iceland with its electrical and heating needs; it also helps with tourism. The geothermal activity of the volcano has created some of the country’s most popular sites.

Most significant of these are Hveragerði town and the adjacent Reykjadalur valley. Hveragerði is often named the ‘hot spring town’ or the ‘earthquake town’ because of the amount of volcanic activity Hengill creates here.

Boiling water runs mere feet beneath the surface of the earth, meaning there are steaming fumaroles all around. Chefs cook simply by burying their food into the earth, leading to an interesting restaurant culture. There is also an exhibition on the town’s earthquake history.

On that note, activity at Hengill has historically caused no end of trouble for the residents of Hveragerði. Though the houses are built to be earthquake proof now, there is little that can be done about the boiling water when it rises. It regularly causes surprise hot springs to rise inside people’s homes.

Reykjadalur can be hiked through from Hveragerði, and is one of Iceland’s easiest, most accessible, and rewarding trails. After walking for an hour or so through a beautiful range of mountains, visitors will come to a river fed by both boiling and rain water.

This mix means that guests can find the perfect points to bathe, based on how warm they want it. The surrounding area is dotted with boiling mud pits and steaming vents.

Hengill is located south of Þingvellir National Park, one of the sites of the Golden Circle. One of the best ways to see the scale of it is to approach the park from Reykjavík, and stop on top of the Almannagjá Gorge.

This gorge runs from north to south, and looking south, there is no missing the slopes of the volcano across the lake Þingvallavatn.

The glacier volcano of Eyjafjallajökull is notorious the world over for causing havoc to air travel in 2010, and stumping television anchors everywhere as they tried to pronounce it. 1651 metres (5427 feet) tall, it is one of the most dominant features of the South Coast.

Geography

The glacier of Eyjafjallajökull is approximately 100 square kilometres (39 square miles), making it the country’s sixth largest. It sits close to the fourth greatest, Mýrdalsjökull, which also conceals another notorious volcano, this one called Katla.

While Eyjafjallajökull’s eruption was huge and disruptive, it pales in comparison to the potential of Katla. Far more explosive, and under much thicker ice, an eruption here in unfavourable wind conditions could have worldwide consequences.

The magma chambers between both of these mighty volcanoes are connected, and, unfortunately for us, an eruption at Eyjafjallajökull is usually followed by one at Katla within a decade.

Eyjafjallajökull has many glacial outlets, the most famous being Gígjökull. Many rivers flow from its meltwater, and one of these falls into the beautiful South Coast waterfall, Seljalandsfoss, which it is possible to fully encircle.

Eruptions

Eyjafjallajökull’s most recent eruption was no doubt the most famous in Iceland’s history (although the honour really should go to Laki, the 1783-4 eruption of which caused an ash cloud so great that Europe fell into a famine that many historians believe led to the French Revolution). On March 27th, 2010, magma began to bubble from beneath the surface, and by April 14th, ash was starting to billow from the peak.

800 people were evacuated, in fears not of magma, but of equally dangerous glacial floods, which have decimated Icelandic towns in the past. Animals were ordered to be kept inside, and those with respiratory problems told they should also stay indoors.

Air travel across Europe was halted, as, by the evening of April 15th, the ash was already over the UK, Scandinavia, and parts of Germany. Holidaymakers were trapped, waiting for news, and would end up stuck for eight days; in Scotland and Ireland, there were even flights delayed in May due to lingering effects.

Thankfully, no one was injured, although the ash is thought to have caused respiratory issues for some in the south of the country. Many farms were also destroyed by the ash and floods, with some farmers still struggling to recover today.

Since settlement in 874, Eyjafjallajökull has also erupted in 900, 1612, and from 1821 to 1823. The latter released a huge amount of fluoride which is believed to have affected the bone health of humans and animals alike at the time.

Eyjafjallajokull today

Eyjafjallajökull is now entirely safe to visit and is seen on most tours of the South Coast in clear weather. In the town of Hvolsvöllur, there is a visitor’s centre on the volcano, which focuses on the experience of one family whose farm, Þorvaldseyri, was one of the many destroyed by the floods, lava and ash.

It is very unlikely that Eyjafjallajökull will erupt again any time soon, with hundreds of years between each eruption, but as mentioned, its neighbour Katla might start rumbling...

Sólheimajökull is an outlet glacier of the mighty icecap of Mýrdalsjökull on the South Coast of Iceland. It is one of the most easily accessible glaciers to reach from Reykjavík, just 158 kilometres (98 miles) away.

For those who are based in Reykjavík, it is by far the favourite spot on which to take guided glacier walks, competing nationally for popularity only with Svínafellsjökull in the south-east.

Geography of Solheimajokull

About eight kilometres long and two kilometres wide (five miles long and just over a mile wide), Sólheimajökull is an impressive feature. Due to the way it descends from Mýrdalsjökull, however, without a clear distinction between the two, it appears much bigger.

Mýrdalsjökull itself has many other outlet glaciers; overall, it is the fourth largest ice cap in Iceland. Beneath its thick surface is one of the country’s most infamous volcanoes, Katla.

The nearby Eyjafjallajökull erupted in 2010 causing widespread havoc at European airports. Throughout history, eruptions in Eyjafjallajökull mean that Katla will also erupt, and so the volcano is due to go off soon. However, volcanoes and all seismic activity in Iceland is highly monitored, meaning that it is perfectly safe to travel around the area and even take an ice cave tour in the glacier above.

Sadly, like all the glaciers in Iceland bar one, Sólheimajökull is shrinking rapidly. A glacier lagoon at its base reveals how quickly it is receding: the length of an Olympic swimming pool every year. It seems like this change is already an irreversible consequence of climate change, and it may be gone within decades.

Visitors to Iceland should, therefore, make sure they witness the ice-cap while it is still with us.

Sólheimajökull has several distinctive traits that separate it from other glaciers. Firstly, it is incredibly easy to find, laying just off of the Ring Road that encircles Iceland. Secondly, it is not surrounded by tall mountains, meaning those who ascend it can attain incredible views of the South Coast. Thirdly, it is home to many walls of ice that can be climbed up with ice axes on certain tours.

There are also crevasses that snake across the surface, spectacular ice ridges and formations, and a vivid colouration that dances between a gleaming white, electric blue, and ash black. Occasionally, you will even find an ice cave, though these can never be guaranteed.

A river runs from the meltwater of the glacier tongue, called the Jökulsá á Sólheimasandi. This river runs through a glacial outwash plain - otherwise known as a black-sand-desert - of Sólheimasandur to the nearby ocean.

Tours on Solheimajokull

Many day tours run from Reykjavík to Sólheimajökull, for glacier hikes or as part of a greater South Coast tour.

Hidden crevasses and ice caves, slippery surfaces, and the threat of rock- or ice-falls all pose dangers on glacier hikes, but glacier guides have to pass several training courses to deal with these eventualities, making the activity quite safe for those in a fit state of health.

All guests are equipped with helmets, ice axes, and crampons, and should arrive wearing warm clothes and sturdy hiking boots.

It is forbidden to ascend glaciers without the correct equipment or training, for your safety and the safety of others. There have been injuries and deaths on Sólheimajökull before, and glacier guides have had to risk their lives to rescue those who flouted the rules.

Reynisfjara is a world-famous black-sand beach found on the South Coast of Iceland, just beside the small fishing village of Vík í Mýrdal.

With its enormous basalt stacks, roaring Atlantic waves and stunning panoramas, Reynisfjara is widely considered to be the most beautiful example of Iceland’s black sand beaches. In 1991, National Geographic voted Reynisfjara as one of the Top 10 non-tropical beaches to visit on the planet.

Reynisfjara is found around 180 kilometers (112 miles) from Iceland’s capital city, Reykjavík, and is a popular stop-off for those taking a sightseeing tour along the popular South Coast.

Driving to the beach is particularly easy, taking an approximate two and a half hours from the capital, so can easily be done within half a day, or a full one combined with other features.

Folklore

Upon visiting the beach, travelers will immediately observe rocky sea stacks sitting off the shoreline, known as Reynisdrangar.

According to local Icelandic folklore, these large basalt columns were once trolls trying to pull ships from the ocean to shore. However, these trolls were dim and went out too late in the night; dawn broke on the horizon, turning the trolls into solid stone.

Another legend tells of a husband whose wife was kidnapped and killed by two trolls. The man followed the trolls down to Reynisfjara where he froze them, ensuring that they would never kill again.

So mesmerizing are these features that they featured in Season 7 of the HBO Series Game of Thrones; you can spot them in a few scenes shot ‘North of the Wall’.

The sea stacks themselves are home to thousands of nesting seabirds. Species that can be found here include puffins, fulmars and guillemots, making it a must-see location for all birdwatchers out there.

Surrounding Sites

Reynisfjara beach is located conveniently in the middle of the South Coast, adjacent to the village of Vík. This means that those taking the Ring Road around the country, or else those heading to the Jökulsárlón glacier lagoon, will pass it, and are encouraged to make a stop.

The closest major landmark is the Dyrhólaey rock arch and cliffs. While many seabirds are found at Reynisfjara, it is nothing compared to the numbers here. From May to August, it is one of the best places to see puffins from land.

Potential Dangers

Visitors to Reynisfjara must be made well aware of the potential dangers present at the beach. First of all, the rolling, roaring waves of Reynisfjara are particularly violent, often pushing far further up the beach than many would expect.

These are called sneaker-waves, and they can appear when least expected, even on incredibly still days. There are no significant landmasses in between Antarctica and the shores of Reynisfjara, meaning waves have thousands of kilometers to build.

Visitors are advised to never turn their back on the waves, and keep a safe distance of at least 30 meters (98 feet).

Aside from these sudden and dramatic shifts in the tide, the rip currents offshore are infamous for their strength and ability to drag helpless people out into the freezing cold open ocean. A number of fatal accidents have occurred at Reynisfjara, the last of which occurred in January 2017.

Vík í Mýdral, or just Vík, is the southernmost village on the Icelandic mainland, located 186 kilometres (110 miles) from the capital Reykjavík.

Often visited by those travelling the popular sightseeing route along the South Coast, it is a wonderful place to stop, recharge, and if you are taking your time, rest for the night. Though it only has around 300 residents, the village is very popular amongst tourists for its convenience and beautiful surrounding landscapes.

Features near Vik

Reaching Vík from Reykjavík takes approximately two and a half hours, and en route, there are many marvellous features to admire. Two of the country’s most famous waterfalls, Skógafoss and Seljalandsfoss, lay between the two destinations; the former has awe-inspiring power, whereas the latter can be fully encircled.

The glaciers Eyjafjallajökull and Mýrdalsjökull can also be seen on clear days; both of these cover volcanoes which are particularly explosive, with Eyjafjallajökull famously disrupting European air travel in 2010. Out to sea in especially good weather, the Westman Islands can also be seen on the horizon.

Just before Vík are the popular birdwatching cliffs of Dyrhólaey, where you can also find an enormous rock arch curving out into the ocean. This is one of the best places for birdwatching in Iceland, with thousands of puffins nesting here from May to August.

The village itself sits opposite one of the country’s most famous features: Reynisfjara black sand beach. Considered one of the world’s most beautiful non-tropical beaches, it boasts incredible geology.

Particularly of note are the Reynisdrangar sea-stacks, said to be two trolls frozen in the light of the morning sun as they tried to pull a ship into shore.

Though this beach makes for a lovely walk, particularly for those staying in Vík overnight, as they can see it under the midnight sun or northern lights, it has its dangers. Sneaker waves can be notorious here, so visitors should stay far from the water’s edge, and never go for a swim. Lives have been lost here before.

The route to Vík from Reykjavík is beautiful and continues to be so as you travel further along the South Coast, through the Skeiðarásandur black-sand-plains into Vatnajökull National Park. This beautiful region is often the final destination of those passing through Vík, as it is home to the largest glacier in Europe, the Skaftafell Nature Reserve, and Jökulsárlón Glacier Lagoon.

Of course, ambitious travellers will carry on from here to encircle the full country.

Wildlife around Vik

Vík, due to its closeness to the Reynisfjall and Dyrhólaey cliffs, has a rich birdlife. Short walks from the village will take you to the nesting grounds of gulls, fulmar, guillemots, and in summer, puffins.

Due to its coastal location, visitors to Vík have a decent chance to see seals on the shore. There is also a slim chance to see whales or dolphins; the twenty or so species that live in Iceland’s waters can appear at any time.

Services in Vik

Vík has a wide variety of public services, due to its remoteness and its importance in connecting the east and west of Iceland. There are gas stations, shops and cafes, a swimming pool, a wool factory that can be visited, and a wide range of accommodation options for all budgets.

Please note, however, that as the village has such a small year-round population, those with special dietary requirements should purchase their food from Reykjavík before departing.